'Once upon a time, long, long ago . . . a geological fairytale'
A once a pun a time geological tale. Everyone can groan loudly at every ‘joke’.
More serious activities can be found on our website.
Monday, 25 December 2017
Monday, 18 December 2017
Festive bauble quiz
Today's new Earthlearningidea, 'Bauble quiz' is fun for all the family and for your class at the end of term.
It's an exercise to consolidate learning about the Earth through comparisons with a festive bauble.
Greeting from the Earthlearningidea Team!
It's an exercise to consolidate learning about the Earth through comparisons with a festive bauble.
Greeting from the Earthlearningidea Team!
Monday, 11 December 2017
ELI activities in the Geopark of Central Catalonia
In November 2017, a presentation of Earthlearningidea activities was made in the Geopark of Central Catalonia. The activities were included as part of the training programme for tourist promoters working within the Geopark.
The photos have been included in the Photo gallery on the ELI website.
There are many activities on the website that can be used for presentations like this one.
The photos have been included in the Photo gallery on the ELI website.
There are many activities on the website that can be used for presentations like this one.
Monday, 4 December 2017
Interpret Earth temperatures from simulated deep-sea and ice cores
The new Earthlearningidea today is 'Interpret Earth temperatures from simulated deep-sea and ice cores' This activity uses sweets to simulate oxygen isotope ratios in cores.
This is an activity to plot Earth’s temperature indications from mock ice and deep-sea sediment cores. The activity consolidates understanding of how the 18 O: 16 O ratios in ice cores and deep-sea cores respectively can be interpreted in terms of warmer (interglacial) or cooler (glacial) Earth temperatures.
More activities relating to climate change can be found on our website.
This is an activity to plot Earth’s temperature indications from mock ice and deep-sea sediment cores. The activity consolidates understanding of how the 18 O: 16 O ratios in ice cores and deep-sea cores respectively can be interpreted in terms of warmer (interglacial) or cooler (glacial) Earth temperatures.
More activities relating to climate change can be found on our website.
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